yo pay ATTENTION in class you dumb a_s_s
Vibrating through movement of rocks
By looking at the rocks and the way the layers of rock are stacked scientist feel they have pretty good idea of the time and severity of many past earthquakes.
No, the rocks in the earth at that depth are too rigid and plastic-like to store the amount of stress needed for an earthquake to occur.
As the sea floor spreads the magnetic orientation in the rocks as they cooled is preserved. As the earth's magnetic field changes then a distinct pattern is imprinted in the rocks. If sea floor spreading is true then this unique pattern should be the same on both sides from the spreading point. Measurements of sea bottom rocks verify this symmetry is true. :)
Earth's interior Plate Tectonics Earthquakes Volcanoes Minerals Rocks
Melting rocks themselves do not directly cause earthquakes. However, the movement of molten rock beneath the Earth's surface, such as in a volcanic system, can create pressure changes that can trigger earthquakes. Additionally, the cooling and solidification of magma can cause rock to fracture, potentially leading to seismic activity.
Vibrating through movement of rocks
Earthquakes
earthquakes
Everything. There is so many ways to change rocks. Erosion by Wind and Water. Earthquakes/Plate Tectonics, Subduction leading to metamorphism and ultimately melting and becoming Igneous. Man.
There are four different types of earthquakes - tectonic, volcanic, collapse and explosion. A tectonic earthquake is one that occurs when the earth's crust breaks due to geological forces on rocks and adjoining plates that cause physical and chemical changes.
Earthquakes happen when under the ground rocks break at a fault. The rocks then break it release of energy which causes semi waves.
Your teacher does not want to hear from some anonymous person on the internet about THEIR school's rocks. Go find some rocks in YOUR area and see if they are being weathered by wind or rain or freezing or earthquakes or chemicals or anything else.
Not pairs ... but sequences. The first shock changes the strain in the rocks, thus often allowing a next quake, followed by yet another one, etc.
aftershocks. These earthquakes can occur hours to years after the main earthquake and are caused by the movement of rocks along the fault line as the earth's crust adjusts to the changes from the initial quake.
The earthquakes are caused by the movement of magma underground and the breaking of rocks by that magma.
Changes caused by weathering and erosion typically occur over long periods of time due to the gradual wearing down of rocks and landforms by natural elements like wind, water, and ice. In contrast, changes caused by earthquakes happen suddenly and are the result of tectonic plate movement, leading to rapid shifts in the Earth's crust. Both processes can alter the Earth's surface, but weathering and erosion are slow and gradual, while earthquakes are sudden and more dramatic.